Direct support and general support maintenance repair parts and special tools lists : pneumatic tires, electric motor, AC, 10 HP, 416V 3 phase, 60 cycle, 50 ft long, conveyor, belt, 300 tons per hr, wheel mounted, 24 in. wide belt, NSN 3910-00-790-2175, Barber-Green model PG 70.

Includes index.

Operator, organizational, field, and depot maintenance manual : conveyor, belt, 300 tons per hr; wheel mounted; pneumatic tires; electric driven; AC, 10 HP, 416 V, 3 phase 60 cycle; 50 ft long; 24 in. belt, (Barber-Greene model PG70), FSN 3910-790-2175.

"July 1961."

Yellow nutsedge : a menance in the Corn Belt /

Bibliography: p. 10-11.

Soil and water conservation research in the Corn Belt States.

"July 1974."

A Ribeira de Iguape,

Mode of access: Internet.

Highway safety : interim report on safety belt and motorcycle helmet effectiveness : report to the Subcommittee on Water Resources, Transportation, and Infrastructure, Committee on Environment and Public Works, U.S. Senate /

"B-243679"--P. 1.

Unit, direct support, and general support maintenance repair parts and special tools lists : conveyor, belt, EMD, 50 ft long, 300 TPH, pneumatic tires (NSN 3910-00-790-2175), Barber-Greene model PG 70.

"June 1992."

Safety belt usage among drivers : use of child restraint devices, passenger safety belts and position of passengers in cars : motorcycle helmet usage /

Final report; May 1980.

Study of methods for increasing safety belt use : comments on the study by the U.S. Department of Transportation, National Highway Traffic Safety Administration /

April 1981.

Preface to peasantry; a tale of two Black belt counties,

Mode of access: Internet.

Development and testing of an airbag and energy absorbing lap belt combination restraint system: final report.

"Contract no. FH-11-6962."

Packing lambda-fold complete multipartite graphs with 4-cycles

A maximum packing of any lambda-fold complete multipartite graph (where there are lambda edges between any two vertices in different parts) with edge-disjoint 4- cycles is obtained and the size of each minimum leave is given. Moreover, when lambda =2, maximum 4-cycle packings are found for all possible leaves.

Volcanic resurfacing and the early terrestrial crust: Zircon U-Pb and REE constraints from the Isua Greenstone Belt, southern West Greenland

The oldest known bona fide succession of elastic metasediments Occurs in the Isua Greenstone Belt. SW Greenland and consists of a variety of mica schists and rare metaconglomerates. The metasediments are in direct contact with a felsic metavolcanic lithology that has previously been dated to 3.71 Ga. Based on trace element geochemical data for 30 metasediments, we selected the six samples with highest Zr concentrations for zircon extraction. These samples all yielded very few or no zircon, Those extracted from mica schists yielded ion probe U/Pb ages between 3.70 and 3,71 Ga. One metaconglomerate sample yielded just a single zircon of 3.74 Ga age. The mica schist hosted zircons have U/Pb ages. Th/U ratios, REE patterns and Eu anomalies indistinguishable from zircon in the adjacent 3.71 Ga felsic metavolcanic unit. Trace element modelling requires the bulk of material in the metasediments to be derived from variably weathered mafic lithologies but some metasediments contain substantial contribution from more evolved source lithologies. The paucity of zircon in the mica schists is thus explained by incorporation of material from largely zircon-free volcanic lithologies. The absence of older zircon in the mica schists and the preponderance of mafic source material imply intense, mainly basaltic resurfacing of the early Earth. The implications of this process are discussed, Thermal considerations suggest that horizontal growth of Hadean crust by addition of mafic ultramafic lavas must have triggered self-reorganisation of the protocrust by remelting. Reworking oft Hadean crust may have been aided by burial of hydrated (weathered) metabasalt due to semi-continuous addition of new voluminous basalt Outpouring,;, This process Causes a bias towards eruption of Zr-saturated partial melts at the surface with O-isotope corn posit ion,, potentially different from the mantle. The oldest zircons hosted in sediments would have been buried to substantial depth or formed in plutons that crystallised at some depth from which it took hundreds of millions of years for them to be exhumed and incorporated into much younger sediments. (C) 2005 Elsevier B.V.All rights reserved.